A NNALES DE L ’I. H. P., SECTION A
G ÉRARD A. M AUGIN
Exact relativistic theory of wave propagation in prestressed nonlinear elastic solids
Annales de l’I. H. P., section A, tome 28, n
o2 (1978), p. 155-185
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155
Exact relativistic theory
of
wavepropagation
in prestressed nonlinear elastic solids
Gérard A. MAUGIN
Universite de Paris VI,
Laboratoire de Mecanique Theorique associe au C. N. R. S.,
Tour 66, 4, Place Jussieu, 75230 Paris, Cedex 05, France
Vol. XXVIII, n° 2, 1978, Physique ’ théorique. ’
ABSTRACT. - The
propagation
of weak discontinuities ingeneral
relativistic
prestressed
elastic solids is studied under the solehypothesis
that the material be
isotropic
inan ideally
unstrained state. No limitationsare
placed
upon theamplitude
of stresses and deformation processes and the formulation hasthermodynamical
foundations. In thisgeneral
frame-work where the state
equation
for thepotential
has aquite arbitrary form,
it is shown that
(i) principal
wave fronts are eitherlongitudinal
or transverse(the propagation
oflongitudinal
onesbeing impeded by
thepossible incompressibility
of thematerial); (ii)
ingeneral,
there may be two transverse waves with distinctspeeds; (iii)
the values of thesespeeds
isexpressible
in terms of three
(scalar)
response functions(typical
of thematerial)
andof the initial
stretches; (iv)
it ispossible
togive
a relative classification of these values and(v)
in the case ofpropagation through
an initial state ofhigh hydrostatic
pressure(case
of dense stellarobjects),
there exists auniversal
relationship
betw een thesimple speed
oflongitudinal
distur-bances and the double
speed
of transverse ones and thespeed
of sound of arelativistic
perfect
fluid that would have a law ofcompression corresponding
to the initial state. For a sensible
special
case of stateequation
and for aninitial state of
hydrostatic
pressure, thespeeds
ofpropagation
and thespeed
of sound referred to above are determinedexactly
in function of twofundamental scalars of the material and a
density
ratio.Taking
accountin
supplement
ofperturbations
in the geometry ofspace-time,
the sameformalism is
applied
to the construction ofperturbation equations
l’Institut Henri Poincaré - Section A - Vol. XXVIII, n° 2 - 1978.
(generalized
Hooke-Navier-Duhamelequations)
valid either for isothermalor
isentropic
processes. The latterequations
are those to be used either in thestudy
of « elastic »gravitational
wave detectors or in thestudy
ofsmall elastic oscillations of dense stellar
objects.
RESUME. 2014 La
propagation
des discontinuites faibles dans les solideselastiques precontraints
est etudiee dans Ie cadre de la relativitégenerate
sous la seule
hypothèse
que Ie materiau soitisotrope
dans un etat idealnon deforme. Aucune restriction n’est
imposee
a1’amplitude
des deforma-tions et des contraintes et la formulation est basee sur la
thermodynamique.
Dans ce cadre
general
ou1’equation
d’etat a uneexpression
suffisammentarbitraire,
il est montre que :(i)
les ondesprincipales
sont soitlongitudi-
nales soit transversales
(Fincomprcssibilite possible
du milieuempechant
la
propagation
despremières); (ii)
il y a engeneral
deux ondes transversales de vitessesdistinctes ; (iii)
la valeur de ces vitesses peut etreexprimee
enfonction de trois fonctions de
reponse
scalaires(typiques
dumateriau)
etdes
elongations initiales ; (iv)
il estpossible
de donner une classification relative de ces vitesses et,(iv)
dans Ie cas ou lapropagation
a lieu dans unetat de forte
pression hydrostatique (cas
desobjets
stellairesdenses),
ilexiste une relation universelle entre la vitesse
simple
desperturbations longitudinales,
la vitesse double desperturbations
transversales et la vitesse du son d’un fluideparfait
relativistequi
aurait une loi decompression correspondant
a l’état initial. Pour uneexpression plausible
de1’equation
d’etat et un etat initial de
pression hydrostatique,
il est alorspossible
dedeterminer exactement les vitesses de
propagation
ainsi que cette vitessesonique
en fonction de deux scalairescaracteristiques
du materiau et d’un rapport de densites. Deplus,
prenant en compte lesperturbations
dela
geometrie
del’espace-temps,
Ie meme formalisme estemploye
a laconstruction des
equations
deperturbation (equations generalisees
deHooke-Navier-Duhamel)
valables pour des processus isothermes ouisentropiques.
Lesequations
ainsi obtenues sont cellesqui
doivent etreutilisees soit dans l’étude des vibrations
elastiques
des detecteurs d’ondesgravitationnelles,
soit dans l’étude despetites
oscillationselastiques
desobjets
stellaires denses.1. INTRODUCTION
In papers
[1 ]-[2] recently published
we have studied thepropagation
of infinitesimal discontinuities in certain
simple
classes of relativistic elastic(or hypoelastic)
bodies. Astudy
of thegrowth
of theamplitude
ofsuch wave fronts
along
their ray has demonstrated the need for an exacttheory requiring
nohypotheses
as far as theamplitude
of strains is concerned andrelying
upon a soundthermodynamics.
It is the purpose of this paperde Henri Poincaré - Section A
to present such an exact
theory
with the solehypothesis that,
in the caseof
arbitrary
finitestrains,
thebody
beisotropic
in anideally
unstrainedstate. The wave
fronts, however,
propagatethrough
aninitially
strainedstate. For
analytical
convenience thestudy
must be limited to that concern-ing
apropagation along
aprincipal
direction of the initial state of stress.Since the state
equations
of the elastic bodies to which the present treatmentapplies
are, for theleast, badly
known(e.
g., in neutronstars),
we concen-trate upon the derivation of those results which may be said to be universal in the sense that
they
do notdepend explicitly
on the exact form of such astate
equation.
Having
recalled some basic notions of thetheory
of deformation processes forgeneral
relativistic matter inspace-time
in Section2,
we establish in Section 3 the exact form of constitutiveequations
for relati- visticisotropic
nonlinear thermoelastic solids.Following
the definitionof infinitesimal discontinuities in Section
4,
we prove in Section 5 a series oflemmas,
theorems and corollariesconcerning
universal(in
the sensespecified above)
resultspertaining
to thelongitudinal
or transverse character of the wavefronts,
the values of thespeed
of these waves, and the relative classification of these values. Ingeneral
two transverse waves with distinctspeeds
and onelongitudinal
wave can propagate. Inparticular,
a universalrelationship
between thepropagation speeds
oflongitudinal
and transversewave fronts in an initial state of
high hydrostatic
pressure(as
may occur in certainastrophysical objects)
is proven in thisgeneral
framework. Thecase of relativistic
incompressible
nonlinear elastic solids whichrequires special
attention isbriefly
commented upon in Section 6 where the non-propagation
oflongitudinal
wave fronts is proven for such bodies. The results arespecialized
in Section 7 for aspecial
form of the free energydensity.
There thespeeds
ofpropagation
oflongitudinal
and transversewave fronts and the
speed
of sound in the case of an initial state ofhydro-
static pressure are determined
exactly
in terms of two fundamental scalars(analogous
to Lame’smoduli),
which are characteristic of thematerial,
and of the
density
ratio.By
way ofconclusion,
we deduce in Section8,
from the exactexpressions
establishedbefore,
thegeneralization
of Hooke’slaw to be used in the treatment of small elastic oscillations either in
« elastic »
gravitational-wave
detectors or inastrophysical objects
actedupon
by
their owngravitational
field. TheAppendices provide
lists ofcoefficients as also a brief
comparison
between constitutiveequations proposed by
different authors for thedescription
of relativistic elasticmatter
( 1 ).
Basic resultsreported
in this paper have been enunciated in ashort Note
[4].
Relatedprevious
worksusing
a differentformalism,
whiche) The brief review given in a preceding paper ([3], Appendix) written in 1971-1972
now is obsolete.
Vol. XXVIII, n° 2 - 1978.
either are based on too
specialized hypotheses
or fall short of the conclusions reached in the present paper, are those of Bressan[5],
Grot[6] (in special relativity),
and Carter[7].
2.
PREREQUISITES
2.1. Notation
Let M =
(V4,
be aspace-time
ofgeneral relativity equipped
witha normal
hyperbolic metric
ga~(x, ~ == 1, 2, 3, 4 ;
index 4time-like ;
Lorentziansignature + , + , + , - ).
ux is thefour-velocity
such that1
(c
= 1 for notationalconvenience). ~~
andoa
denote thepartial
and covariant derivatives with respect to the local chart x03B1 of M.D =
u03B1~03B1
is the invariant derivative in the direction of M".P03B103B2
= g03B103B2 + u03B1u03B2 is thespatial projector
which is usedsystematically
in thefollowing
deve-lopment
to write down the local canonicalspace-time decomposition
ofany tensor field defined on M. The local
spatial projection
of anygeometrical object
A is notedA1
and admits u as zero vector for all its indices in a local chart.Objects
such that A =A1
are said to bespatial.
The transverse orspatial
covariant derivative is definedby oa
=22 Deformation of matter in
space-time
Following Maugin [8]
and Carter andQuintana [9],
we admit that the motion of a relativistic continuum is described eitherby
means of a canonicaldifferentiable
projection P
such that P :G[B] ~
N or with the aid of thespace-time parametrized
congruence of world lines ~ : x =~(X, T),
X E
B,
1" e !R. HereF[B]
is the open tube of y4 which is swept outby
thematerial
body
B(whose
constituents are the material «particles » X)
and
(V3, K,
L =1, 2, 3,
is the three-dimensional manifold which serves to describe the material continuum. B is an openregion
of T is the proper time of X. ~ is
equipped
with the localbackground
metric
GKL
and local chartsXK,
K =1, 2,
3. We have thusThese relations are assumed to possess a sufficient
degree
ofcontinuity
and
differentiability
in their arguments so as to allow for theforthcoming manipulations.
Forinstance,
one can define the inverse motiongradient X~
by
°‘~ being
thereciprocal
of aspace-time
invariant notedC L
buttensor field on ~~~ 2014 is constructed
by applying
theprojection ~ :
Annales de l’Institut Henri Poincaré - Section A
This defines the relativistic
analogue
of the Piola finite-strain tensor of classical continuum mechanics(Compare [lO], Chap. I).
Itsgeometrical significance
is clear. It is theimage
of thespace-time
metricby
theprojection
of thespace-time
on itsquotient by
the congruence(2.1)3’
Furthermore, assuming
that the Jacobian determinant of(2 .1 )3 keeps
the same
sign (e.
g.,plus)
in the course of the relativistic motion of X anddefining
the direct motiongradient xK by
the chain rule of differentiation
yields
and it is
possible
to define the strain tensorCKL
such that =ði
and
Let
Gxa
be theimage
ofGKL
in Mby f!JJ, i.
e.,Then we can define two useful tensor fields which serve to measure finite strains either on N or on M,
EKL
and such that[3] [77] ]
and
Elementary computations [3], [72]
then allow one to establish thefollowing
results that relate
propertime
rates ofchange
of differentgeometrical objects
of interest :and where
and
Vol. XXVIII, n° 2 - 1978. 11
for any
spatial
tensorAaa
= denotes the Lie derivative with respect to the field u. In terms of the differentiableprojection 9,
we haveEquation (2 .12)2
is a consequence ofEqs. (2.12)i, (2 . 7)
and(2.10).
Thisshows that
G«~
is thebackground
metric onM,
which serves as a local standard to measure strains.According
toEqs. (2.12)
and(2.14),
theHerglotz-Born
local condition ofrigid-body
motion is defined in diffe- rential form(Killing’s theorem) by
either one of thefollowing
conditions :2.3. Field
equations
In
supplement
to Einstein’s fieldequations
that relatelinearly
theEinstein tensor and the total energy-momentum tensor, we have
Here
p(x)
=p(X, T)
is the mass per unit of proper volume. In absence of heatconduction, electromagnetic
fields andspin
the energy-momentumtensor admits the
following simple
canonical space-time decomposi- tion :where t03B103B2 = t03B203B1, as a consequence of
Eq. (2.20)2,
is thespatial
relativisticstress tensor, and E is the internal energy per unit of proper mass.
Taking
account of
Eq. (2.19)
and of the fact that =0,
weproject Eq. (2.20)i along
u~ andorthogonally
to u to obtainand where
is the tensorial index of the
continuum,
cf. Ref.[2].
In the present case the local statement of the secondprinciple
ofthermodynamics
reduces to theequation Dry
=0, where ~
is the entropy per unit of proper mass.Introducing
the
specific
free energyt/J by
= s 2014 where 8 is the proper thermo-dynamical
temperature(o
>0,
inf 8 =0),
we can rewriteEq. (2.22)
inthe form
Annales de l’Institut Henri Poincaré - Section A
3. CONSTITUTIVE
EQUATIONS
FOR ISOTROPIC THERMOELASTIC BODIES
A natural definition for
general
thermoelastic bodies(i.
e., with apriori large deformations)
isgiven by postulating
a functionaldependence
of theform
.
That
is,
there are nohereditary
effects sincedependent
andindependent
variables are considered at the same event
point
of M or,equivalently,
for the same values of the four parameters
(XK, -r).
Then we have theTHEOREM 3 .1. - The exact constitutive
equations o, f ’
ananisotropic
thermoelastic
body
aregiven by
03C8 satisfying
0 thefollowing
0 setof first
order linearpartial differential
tions:
It then follows the
L __
COROLLARY 3.2.
Equations (3.2)
and(3.3)
can bereplaced by
i. e., the image by P
of TKL ~ (~03C8/~ Ch) = TLK
up to the2014
Consider ~
=0)
to startwith,
then compute with thehelp
ofEq. (2.10)i
to obtainif c~ =
Furthermore, according
to theprinciples
of formulationset forth
by
theAuthor, 03C8
must beobjeetive,
i. e., itsexplicit
form shouldnot
depend
on the observer[12], [l3].
We have shown that in the presentcase which does not involve
hereditary effects,
this invariance isequivalent
to the rotational Lorentz invariance of
L~
in a local inertialframe,
orelse,
to invariance under all generators ofSO(3)
in local nonholonomicspatial
framesalong
~.Studying
such a form invariance for8)
underinfinitesimal
transformations xa ===
+ inspecial relativity
orunder infinitesimal rotations = =
1, 2, 3,
betweenrigid
Vol. XXVIII, n° 2 - 1978.
spatial
triads at an eventpoint
ofM,
where * indicatesvalidity
ininertial frames
only,
e is aninfinitesimally
small andL~a
isarbitrary,
andrecasting
theresulting equation
in acomplete
covariantframework,
we are led to the condition(3 . 3).
On account ofthis, Eq. (3.5) simplifies
and theexpression
of03C1D03C8 being
carried inEq. (2.25)
which isposited
to be valid for any DB and all deformation fields that do notrigidify
the continuum in the sense of
Herglotz
and Born(i.
e.,0), completes
the
proof
of Theorem 3.1. The system of differentialequations (3.3) integrates immediately along
its characteristics if~ depends
onX~ only through
thespace-time
invariant combination Hence theproof
ofCorollary 3.2; Q.
E. D.Equations (3.4)
are theequations
deduced pre-viously
from a variationalprinciple by
the Author[8].
Equations (3.4)
and thoseequivalent equations
which are discussedin
Appendix
I describeanisotropic
thermoelastic bodies. The notion of material symmetry which relies uponcristallography
isessentially
a three-dimensional Euclidean
notion,
i. e., it concerns thestudy
of the invarianceof functions with respect to members of
subgroups
of the group0(3).
Since,
as a result ofCorollary 3.2, ~r depends
nowonly
on arguments defined on 8being
a parameter, material symmetry must be discussed in the local tangent space to ~l at X.However,
we shall avoid thiscompli-
cation in the
sequel
for we shall useonly
arguments defined on M to faci- litate theanalysis
of wave-frontpropagation.
Infact, using
the resultenunciated in Theorem
3.1,
we can state theTHEOREM 3.3. -
a)
The exact constitutiveequations of’
anisotropic
relativistic thermoelastic
body
aregiven by
eitheror
depending
onwhether ~
or E is used asthermodynamical potential.
b)
and B areisotropic functions [in
the sense ’ ofSO(3)]
of
therelativistic finite-strain
tensor ~.Proof
2014 Wecan write Eq. (2.9)
in the formNote that
depends
onX~
viaX~
itself and viaCMN
thatdepends
on~
hence on its
reciprocal X~ .
It followsby varying Eq. (2.5)i
1 thatAnna/es de Henri Poincaré - Section A
From
Eq. (2.6)
it follows thatThen
Eq. (3.8) yields
on account of
Eqs. (2.5). Then,
if one makes thechange
ofindependent
variables
~(X~0) ~ Eq. (3.11)
substituted inEqs. (3.2)i
and
(3 . 3) yields Eq. (3.6)1 and,
on account of the symmetry of thefollowing
system of first order linearpartial
differentialequations
similar
equations involving 8
insteadof 03C8
are obtainedby performing
the
partial Legendre
transformation e= ~
+ As isreadily checked, Eq. (3.12)
is but the covariantexpression
of the factthat ~
must beobjective,
i. e., form-invariant
by SO(3)
in a local inertial frame. In such a frameEq. (3.12)
is satisfiedidentically if 03C8 depends
on Eonly through
its funda-mental invariants
Ik
= tr~k,
tr =trace, k
=1, 2,
3. Since these are space- timeinvariants,
the result holdsgood
infully
covariant formalism. Thismeans
that 03C8
or E is anisotropic
function of its tensorial argument, 8 or ~acting
as asimple
parameter. Thebody
thus described exhibits nopreferred spatial
direction as far as its response to deformations is concerned. It isisotropic ; Q.
E. D.Applying
theCayley-Hamilton
theorem it then ispossible
to restate theforegoing
result asCOROLLARY 3.4. - The exact constitutive
equations of
anisotropic
relativistic thermoelastic
body
aregiven in
intrinsic notationby
where the
gr’s
arespace-time
invariant scalarsand, by
convention,(~°)°‘a =
On account of the
expression given
inAppendix
II for the scalars gr,Eq. (3.13)1
is the relativistic version of the constitutiveequation
derivedby Murnaghan [l4]
in classicalisotropic elasticity
with finite deformations.Remark that this
equation
is universal in the sense that 8 is ageneral
func-tion of the invariants
Ik,
whoseexpression
can be constrainedonly by
someregularity assumptions,
some conditions of elasticstability
and the condi-tions of relativistic
causality
and therequired reality
of wavespeeds,
thelatter
being
determined infollowing
sections.Vol. XXVIII, n° 2 - 1978.
Remark.
2014 (f)
The manner in which theequations
above have been obtained guarantees thatthey
are valid inspecial relativity,
and at thenonrelativistic
limit,
in classical continuummechanics,
andthat,
insupple-
ment to the
objectivity requirement
of theAuthor, they satisfy identically
the
rheological
invarianceproposed by Oldroyd [15]
forgeneral
relativistic continuous matter.Remark.
- (ii)
A directproof
ofEqs. (3.13)
can begiven by starting
with the a
priori
functionaldependence ~(~ap, 8). Then,
incomputing
one uses
Eq. (2.16)
to pass from to hence todaa
in virtueof
Eq. (2.14). Taking
account of thedecomposition
of ea~ insymmetric
and
skewsymmetric
parts, one is thus led toApplying
the same argument as thatapplied
in theproof
of Theorem3 .1,
but for theobjectivity of 03C8
as a function of it resultsEq. (3.12).
HenceEq. (3.14) simplifies,
and it remains to substitute for theexpression
ofprovided by
thissimplified equation,
intoEq. (2.25)
to arrive at theresults
(3.6).
4. DEFINITION
OF INFINITESIMAL DISCONTINUITIES
We recall the definitions introduced in a
previous
work[16] (See
alsoLichnerowicz
[77]).
Let = 0 be the time-likehypersurface
that represents adiscontinuity
front which propagates in V4 and thus separates~ _
F[B]
in twosubregions
and at each time. We setand
~ is the
(nondimensional) speed
of thediscontinuity
front measured relati-vely
to themoving matter. l"
is oriented from the « minus » to the «plus »
side of W. A + and A -
being
the uniform limits of A inapproaching
W onits two
faces, we note [A] =
A+ - A-. IfA,
g03B103B2 and u03B1 are continuousacross Wand
if 03B4
denotes the Dirac distribution with compact supporton
W,
then we can write -and
where ’ the field ðA is called the infinitesimal
discontinuity
of Athrough
W.We call the
two-plane
’orthogonal
to the unitspatial
vector,
Annales de l’Institut Henri Poincare - Section A
S«~ = P«~ - !~«~’~,a
is the covariantprojector
on toH~~.
The canonicaldecomposition
of anyspatial geometrical object along
the direction of ~, and on toH~
is obtainedby applying
the operatorS,
e. g., with an obvious notation and obviousproperties
for the elements ofdecomposition
thusintroduced,
Similar
decompositions hold good
forf«~
and with the elements ofdecomposition F«, F)
andE«, E), respectively.
We call
Ø’[B]
cM) == {p,
~, 17, u«, a solution of thesystem of
equations
formedby
Einstein’s fieldequations, Eqs. (2.19)
and
(2.23),
the constitutiveequations (3 .13)
and the conditionD17
= 0(provided
that such a solutionexists;
this difficultproblem
of existence is notapproached
in thispaper).
Then the wave fronts that we consider in theforthcoming
sectionssatisfy
thefollowing
set ofhypotheses :
Hi :
anytypical
solution is continuous acrossW;
H2 :
except for the metric allspace-time
derivatives of the first order of the fields of the solution suffer discontinuities across W(the
case where 0
requires
aspecial study);
H3 :
W is not agravitational
wavefront,
i. e., ~2 - 1 isexcluded;
.H4 :
W is not a material wave front or, in otherwords,
sinceD17 = 0 yields ~~~
= 0 in agreement withEq. (4.5)~,
W is not an entropyfront,
i. e., ~ = 0 is excluded so that
~r~
= 0necessarily.
In virtue of
H..1,
W is not a shock wave since~u«~ ~
0. In virtue ofH3
and
H4
the admissible range for GlC is limited to the open interval]0,1[ c= ~
if ~ is to be real and less than the
light velocity
in vacuum(relativistic causality).
We call
principal
wave fronts those wave fronts forwhich ~,«
coincideswith an
eigenvector
of the initial state of stress EAccording
toEq. (3.13)i,
if W is such a wavefront,
then thecorresponding ~,«
coincidesalso with an
eigenvector
of the initial state of strain ENaturally,
this holds true
only
forisotropic
bodies.Longitudinal
wave fronts are thosewave fronts for which
(~u ~ 0, ~u1
=0),
and transverse wave fronts arethose for which
(5M
=0, 0).
We shall not considergeneral
wavefronts which may be called mixed wave fronts
(Cf. [2] ).
5. PRINCIPAL WAVE FRONTS
IN ISOTROPIC RELATIVISTIC THERMOELASTIC BODIES We consider
only principal
wave fronts except indegenerate
cases ofinitial state of stress where the character or
principalness
has nomeaning.
In
general
admits three distinctorthogonal (with
respect to the metriceigenvectors (spatial
unitfour-vectors) ~=1,2,3,
Vol. XXVIII, n° 2 - 1978.
with
corresponding eigenvalues ~.
For aprincipal
wave frontW,
letd~ 1,
coincides with A.
d~ 1 ~
is also aneigenvector
of Lett{ 1 ~
be the
corresponding
stresseigenvalue and E~
thecorresponding
straineigenvalue. Then t~
andE~
are relatedby
theequation
The
remaining
twoeigenvectors
of bothta~
and andd~3~,
form anorthonormal
dyad
on which can beprojected
any tensorialobject
A suchthat
S(A)
= A. Then we can set thefollowing
lemma.LEMMA 5.1. -
Principal (infinitesimal discontinuity)
wavefronts
Wthat
propagate in
anisotropic
relativistic thermoelasticbody
are eitherpurely longitudinal
orpurely
transversal.Proof.
Astraightforward
calculationyields
thefollowing expression (written
in intrinsicformalism)
for theright-hand
side ofEq. (2.23)
onaccount of
Eq. (3.13)1 :
where
gr(Ik, ~) -
and the nine scalars which are functionsof
Ik and ~ only,
are listed inAppendix
III.Now consider the infinitesimal discontinuities of
Eqs. (2.19), (2.23)
and of
(~~
on account of the definition(2.16)
and ofEq. (5.2). Taking
account of the fact that
fa~
and are continuous across Wandusing
thedefinitions
(4.1) through (4.5)
andEq. (5.1),
weobtain,
with ~ ~0,
and
Annales de l’Institut Henri Poincaré - Section A
where
n writmg /) we nave taken accoum 01 me results (5.5), (5. 5) anu
(5.6)
and of the fact that51]
= 0.Upon using
thedecompositions (4.6)
and
(4. 7)
and theanalogous decompositions
forfa~
and~a~
andaccounting
for the fact
that, being
aneigenvector
of and it also is aneigen-
vector of the
projection
ofEq. (5.7) along
the direction of Ayields
~’ F - {(1 - 2~)~ - ~
+2~~1)
+2~(1 - 2~)} ~~u = 0, (5 . 9)
with 2
whereas its
projection
onto readsthe mixed
projection vanishing identically
forfa
=Fa
=Ea
=0 ;
hencethe
proof
of Lemma 5 .1. Thatis,
we haveuncoupling
betweenlongitudinal
and transverse wave fronts because
(i)
of theisotropy
of thebody
and(ii)
of the
principalness
of the wave front.Since
p ~ 0,
we can state at once thefollowing
theorem :THEOREM 5.2. -
Longitudinal principal
wavefronts
thatpropagate in
an
isotropic
relativistic thermoelasticbody
have aspeed
such thatwhere
is the
principal
stretch in thespatial
direction whereas transverseprincipal
wave
fronts
ingenerat
have two distinctspeeds, uT2
anduT3,
which areso utions
0
theequation
where
Equation (5.14)
is solvedimmediately
in the nonholonomic frame(d(2~,
where
diagonalizes. Setting .f’2
=F.2, 3
=F?3, ~2
=E.2, ~3 = E33,
and i;, =
( 1 - 2~)’~~ ~’
=2, 3,
the solutions of(5.14)
aregiven by
Vol. XXVIII, n° 2 - 1978.
For the wave
speeds
to be real and less thanunity,
theright-hand
sideof
Eqs. (5.12)
and(5.16)
must be in the interval]0,
1[.
Thisclearly imposes
constraints on the initial state
9Mo
i. e., on rathercomplex
combinations of the response functions gr and the initial strains andstretches,
and vk.Apart
from thoseconstraints,
the results enunciated in the form ofEqs. (5.12)
and(5.16)
are universal sincethey
do notdepend
on any assump- tion asregards
theamplitude
of strains(e.
g.,they
are validfor finite strains)
and on any
particular
functionaldependence
of the internal energy E(Ik, ri),
which of course possesses a sufficient
regularity.
Ageneral study
of theconstraints referred to above cannot be
performed
under thehypothesis
ofa
general
initial state. Neither can it be achieved a relative classification of the two transverse wavespeeds
in an exact manner in such ageneral
frame-work. The
approximate following results, however,
can be established.Let us define
Ak, k
=2, 3, by
Then with the definition
of vk
we cangive
thefollowing
form to the diffe-rence
~T2 - ~3:
Of course,
f2 ~ /3 ==
1 +0(c-2)
>0,
so that we can introduce a meanvalue f
forf2 and f3
and rewrite(5.18)
asThe
Ak
are allpositive
from their verydefinition,
and vi > v~yields Ai A~.
We have thus
COROLLARY 5.3.
- a)
Transverse wavefronts
withamplitude paraltet
to the axis
of
lesser transverse stretch travel at a greater absotutespeed
than others
if,
with gl 1 >0,
i)
either g2 0 and 1 -f(A2
+A3) g1/g21, ii)
Or g2 > 0 andf(A2
+A3) -
1b)
Transverse wavefronts
withamptitude parattel
to the axisof
greatertransverse stretch travet at a greater absotute
speed
than othersif,
with gl >0, i)
either g2 0 and,f’(A2
+A3) -
1g1/g2,
ii)
Or g2 > o and 1 -(A2
+A3) g1/g2 I
c)
The two typesof
wavefront
travel at the same absolutespeed if
andonly if
thecorresponding
transverse stretches areequal.
The result
c)
is exact and does notrequire
theapproximation (5.19).
Statements
a)
andb)
follow from the discussion of thesign
of theright-
hand side of
Eq. (5.19).
The reason
why
we have considered gl > 0 is made clear as follows.Another
possibility
forexpressing
the difference~T2
--~T~
is obtainedAnnales de l’Institut Henri Poincare - Section A
by reintroducing
theprincipal
stressest(2~
andt(3~
via anequation
ofthe
type
ofEq. (5.1)
for thosequantities
in terms of theeigenvalues ~2
and
~3.
We haveand
Hence, Eq. (5.20)
takes the formif
where
is Lame’s modulus and CT is atypical
transverse-wavespeed.
g 2’ == 0 represents one part of the neo-Hookean
assumption (stress-strain
constitutive relation at most
explicitly
linear inF). Equation (5.23)
issimilar to an
equation given
in ourprevious
work[2].
It says that transversewave fronts with
amplitude parallel
to the axis of lesser transverse stress travel at a greater absolutespeed
than the others. The other part of the neo-Hookeanassumption
is obtainedby looking
atEq. (5.18) which,
withthe
approximation
madeabove,
takes the same form asEq. (5.23)
if andonly 03C1g1/2v2,
where v is atypical
transverse stretch.Since
isexperi- mentally
shown to bepositive (and
must in fact be soaccording
to thethermodynamics
of neo-Hookeanmaterials),
andv2
>0,
then gl must be greater than zero.By
the same token the definition(5 .24)2
makes sense.In conclusion of
this, point
arepresentation
of neo-Hookean materials is obtained forThe statement
c)
ofCorollary
5.3 holdsgood
in certaindegenerate
cases of initial stresses and
strains,
forinstance, i )
if this state is acylindri- cally symmetric
one about the direction andii)
if this initial state isspherical,
thatis, fully degenerate,
in which case the above-obtained resultsapply although
the notion ofprincipalness
has lost itsmeaning.
Such aninitial state
is,
forinstance,
an initial state ofhigh hydrostatic
pressure, ascan arise in the «
geophysics »
of neutron stars(See
Ruderman[7~]). Regard- ing
thisspecial
case thefollowing
remarkable result can be arrived at.THEOREM 5 . 4. -
(simple) speed u~ and the (double) speed 0, f longitudinal
and transverse wave.f’ronts
thatpropagate in
anisotropic
relativistic nonlinear elastic
body, of
which the initial state is oneof high
Vol. XXVIII, n° 2 - 1978.
hydrostatic
pressure po(case of
dense stellarobjects),
are relatedby
theuniversal
relationship
,^
where
and
a
being
the soundspeed,
andf
the index(in
the sense ofLichnerowicz), of
a retativisticperfect fluid
that would have the same tawof compression.
~’roof.
We are in afully degenerate
case for whichwith
where ~~! = C2
= C. Set v =( 1 - 2~) -1 ~2
theisotropic
stretch in the state9Ko.
Then the matter properdensity
and the samedensity
in an
ideally
unstrained state, p~i~, are relatedby
theequation
= 3.We deduce thus
and
by applying
the chain rule of differentiation. It follows from(5.30)
and(5.32)
thatwhereas
Eqs. (5.12)
and(5.16)
reduce toand
respectively,
on accountof Eq. (5.31)
and o of the definition(5.28)1.
Substi-Anna/es de l’Institut Henri Poineare - Section A
tuting
from(5. 33)
into(5.34)
andcombining (5. 34)
and(5. 35) completes
the
proof. Q.
E. D.The exact result
(5.26)
valid within the relativistic framework of finite- straintheory
is universal for nohypotheses
need be madeconcerning
theexplicit
functional form of the internal energy function. It consists in thegeneral
relativisticgeneralization
of a classical result due to Truesdell[19].
In the neo-Hookean case described
by Eq. (5 . 25)
it reduces to theequation proposed by
Carter[7].
It is reasonable to assume that > 0.Therefore,
ingeneral, ~ ~2 ~~ > - Relativistic causality
thus imposes
that
(4/3)~lCl
+ 1. That is,
It is difficult to establish the
reality
of but thefollowing
can bepointed
out :
COROLLARY 5.5.
- If
transverse wavefronts
can propagate at all inan
isotropic
retativistic nontinear elasticbody in an
initialstate of hydro-
static pressure, then
longitudinal
wave.f’ronts
can propagate as welt.Indeed,
ifu2|
>0,
thenU2~
>a2
> 0.However,
ifU2|
0(no
propaga- tion of transversefronts),
then~~~
a2 and~~~
can be zero orimaginary,
so that the case
~~j
0(no propagation
oflongitudinal
wavefronts)
cannot a
priori
be excluded.In the neo-Hookean case the
causality
condition(5.36)
takes on thesimple
form(with
=EFor a
body
unable to supportshearing effects,
hence for,u
=0,
this lastinequality
reduces to thatgiven
in relativistichydrodynamics (Cf.
Israel [20] ).
6. REMARK ON THE INCOMPRESSIBLE CASE
Typical
materials for which theforegoing development applies
are thosewhich make up the thick crust of neutron stars, of which the outer
portion probably
resembles terrestrial matter except that it is about1018
times morerigid
than steel and much moreincompressible,
so that it is easier tojiggle
it than to compress it
(Cf. [8], [21 ] ).
Conclusionsregarding
thislimiting
case can be drawn
directly
from the results ofprevious
sections. If the relativistic elasticbody
isincompressible,
then the deformations it suffersare isochoric. This is
expressed
in terms of the strain tensorby
thecondition
Vol. XXVIII, n° 2 - 1978.